Archive image from page 240 of Description, analysis and predictions of. Description, analysis and predictions of sea floor roughness using spectral models descriptionanaly00foxc Year: 1985 -1000 a m-'- i.''-' £ - -0â0 5ââ ' 0 ° U-20 '1âIâIâiâI 1âI 1âIâI 1âIâI 1âI 1 r 20 la 60 80 100 120 140 160 180 AZIMUTH (degrees) Figure E-3 Artificially generated surface composed of two orthogonal trends with identical intercepts of a= , but spectral slopes of b= in the N-S direction and b= in the E-W direction. Azimuthally dependent spectral parameters are plotted below
Archive image from page 240 of Description, analysis and predictions of. Description, analysis and predictions of sea floor roughness using spectral models descriptionanaly00foxc Year: 1985 -1000 a m-'- i.''-' £ - -0â0 5ââ ' 0 ° U-20 '1âIâIâiâI 1âI 1âIâI 1âIâI 1âI 1 r 20 la 60 80 100 120 140 160 180 AZIMUTH (degrees) Figure E-3 Artificially generated surface composed of two orthogonal trends with identical intercepts of a= , but spectral slopes of b= in the N-S direction and b= in the E-W direction. Azimuthally dependent spectral parameters are plotted below. 208
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